Global Volcanism Program | Hekla 09/2014 (BGVN 39:09) Elevated seismicity during March-April 2013 Information is preliminary and subject to change. All times are local (unless otherwise noted) May 1970 (CSLP 43-70) Eruptions and lava fountaining from multiple fissures starting on 5 May Card 0933 (07 May 1970) Eruption from fracture system; tephra fall to the N The following telephone report from Hiynur Sigtryggsson of the Icelandic Weather Bureau was relayed . . . by Paul Bauer. "At approximately 1800 EDT (2200 GMT) on 5 May 1970, the volcano Hekla blew up and is now in eruption." The following report from the National Research Council of Iceland was relayed . . . by Jules Friedman. "There is an eruption from the fracture system controlling Hekla. There are two outflow centers active at the present time, one is said to be N of Hekla, the other S of Hekla.

Aparently short cross fractures across the main Hekla fracture system are involved. There was, at least yesterday (5 May) and possibly continuing today, an eruption cloud. According to reports here in Washington last night, the eruption cloud deterred light aircraft and prevented any more detailed observation. In a sector N of the volcano, there was a tephra fall, tephra used in lieu of ash to indicate different size fragments. The wind sector is pointed N so that this is the area affected by the ash fall, and some farms were being evacuated." Card 0934 (07 May 1970) Inspection flight reveals 13 vents and fissures; dense ash cloud to 29,000 feet The following report from the Iceland Defense Force was passed to the Center by Commander Bolst. "Reporting from the Commander Iceland Defense Force. Time of the report is 061140 Zulu of May 1970. Due unfavorable weather and danger from flying rock and pumice cloud, P3B aircraft, volcano reconnaissance flight, was directed to remain outside of ten miles with minimum altitude of 10,000 feet.

Nevertheless, crew managed to observe the eruption area for about 20 minutes before weather closed in entirely. Apparently there are seven fissure vents along the southeastern slopes of Mount Hekla proper. These had emitted an estimated 4 square miles lava flow. An eighth vent was observed on the NW slope, the peak itself obscured by clouds and smoke. About four miles, bearing 070° from peak, five additional fissures also violently emitting fire and rock but no lava. Latter are not associated with peak or any existing crater but are on relatively flat lava plain. All 13 vents and fissures were emitting fire to an altitude of 500-1,000 feet, and dense ash and smoke were observed to 29,000 feet. Local reports indicate pumice fall and lava flow now subsiding. As area is relatively sparsely settled, Icelanders have accomplished the required evacuation and have situation in hand." The following cable was received from S. Thorarinsson on 7 May.

"Inspection Hekla area reveals eruption not in Hekla proper but separate fissure eruptions with very high fountains N, SW, and S of Hekla." Card 0936 (11 May 1970) Present activity mainly lava with some pumice production The following cables were received from H. Sigtryggsson. "Seismic activity recorded Reykjavik began at [2058 on 4 May] with irregular tremors generally increasing until [2200 on 5 May] but subsiding considerably after [2235] and virtually disappearing around midnight. Several earthquakes recorded, first one at [2058 on 5 May] largest at [2140, M 4] last earthquake at [0203 on 6 May]. No seismic activity observed since. Eruption activity first observed [2133 on 5 May] explosive at first with moderate pumice production depth of pumice layer close to 8 cm, 15 km from volcano. Explosive activity decreased after midnight and lava flow became predominant. Eruption cloud initially reached height of about 15 km, initial cloud drifted NNW.

Moderate lava flow has reached length of about 2 km. Nuees ardentes not observed. No activity has been observed at the main crater of Hekla, activity mainly confined crater groups about two kilometers to NE of summit crater. present activity mainly lava production with slight pumice production." "Further information on Hekla eruption. Lava eruption continues with slightly diminished intensity. Sickness of livestock possibly due to effects of volcanic ash or other effects of the eruption have been reported at some farms near the volcano." Card 0940 (14 May 1970) Summary of fissure locations and activity; high amounts of fluorine A flank eruption of Hekla occurred shortly after 2100 local time on 5 May. The erupting fissures were at oblique angles from the main Hekla fissure system running very nearly N to S (12° to the E). Initial lava fountaining reached heights of 700-800 m within three hours after the eruption began. The most violent vents were on the SE side of Hekla, four fissures erupted.

The first fissure is located on the W flank 2,500 m from the summit and 150 m in length. The second fissure is located 3,000 m to the N of the summit with a length of 400 m at an elevation of 400 m. The third and fourth fissures are located on the SW flank; one at an elevation of 800 m and the other at an elevation of 700 m. They have lengths of 50 m and 700 m respectively. There was some change in lava composition during the first two days. The first ash produced by the eruption contained 8.65% Fe2O3, and the first lava contained 9.3% Fe2O3. Stronium was 310-350 in the same sequence. Ten square kilometers of surface area were covered by lava during the first 24 hours of the eruption. After the second day the surface area covered by lava has not substantially increased but the thickness of the lava has increased. Total volume of lava is estimated to be 0.5 km3 by 12 May.

Total volume of tephra is estimated to be 0.2 km3 by the same date. Seventeen cm deep ash was recorded 10 km from the volcano's summit on the axis of the ash fall. One-half cm deep ash was recorded 300 km from the volcano summit. Local groundwater is measuring high amounts of flourine, which is toxic to sheep and horses. Fluorine concentration in creek water has been measured at 10 mg per liter. Eruption cloud recorded on radar reached a height of 53,000 feet on 5 May. By 12 May the S and W craters had come to a complete stop. The W vent stopped on 7 May. The S vent stopped on 9-10 May. The N crater continues activity at a considerably reduced level. Card 0944 (22 May 1970) New fissure on 20 May has 20 lava fountains The following cable was received from Dr. Sigurdur Thorarinsson on 22 May 1970.

"At 2240 on 20 May, a 1 km length fissure opened up one km further N of northern crater of Hekla volcano. The new fissure direction is NE-SW with 20 fountains playing. Lava flow considerable." Information Contacts: Card 0933 (07 May 1970) Icelandic Weather Bureau via Paul Bauer, American University, Washington, D.C. USA; National Research Council of Iceland via Jules D. Friedman, U.S. Geological Survey. Card 0934 (07 May 1970) Commander, Iceland Defense Force via Lt. Cmdr. Bolst, U.S. Navy, Norfolk, Virginia, USA; S. Thorarinsson, Icelandic Museum of Natural History. Card 0936 (11 May 1970) Hlynur Sigtryggsson, Icelandic Weather Bureau, Vedurstofa Islands, Reykjavik, Iceland. Card 0940 (14 May 1970) S. Thorarinsson, Icelandic Museum of Natural History; G.E. Sigvaldason, Science Institute, University of Iceland.

Card 0944 (22 May 1970) S. Thorarinsson, Icelandic Museum of Natural History. July 1970 (CSLP 43-70) Eruption ends on 3-4 July; area of fluorine poisoning is clearing Card 0974 (20 July 1970) Eruption ends on 3-4 July; area of fluorine poisoning is clearing The eruption came to what is likely to be a definite end during the night between 3-4 July. In the areas in North Iceland most seriously affected by fluorine poisoning, so much of the fluorine has been washed away from the ash that the grazing grounds are regarded as tolerably safe for grazing. Information Contacts: Sigurdur Thorarinsson, Science Institute, University of Iceland.

January 1971 (CSLP 43-70) Review of May-July 1970 eruption Card 1093-1094 (19 January 1971) Review of May-July 1970 eruption The eruption commenced at 2123 ± 2 minutes on 5 May 1970, and lasted until 5 July, or exactly two months. The real Hekla fissure, which splits the Hekla ridge lengthwise, did not open up this time except in its extreme SW. The main eruption was from fissures at the base of the Hekla ridge to the SSW (Sudurgigar), and NE (Hlidargigar). The eruption in the Sudurgigar began at an elevation of about 800 m above sea level. The elevation of the highest Hlidargigar, where eruption began about an hour later than in Sudurgigar, is about 640 m. During the first phase of the eruption, the eruption cloud reached 15,000 m height.

The main tephra fall lasted about two hours, during which time the tephra production averaged 10,000 m3/sec. The total volume of the tephra produced was about 70 million m3. The bulk of the tephra came from the Sudurgigar crater row SSE of the Hekla ridge. The tephra was carried NNW and reached the north coast of Iceland, 90 km from Hekla, in 2.5 hours. The tephra sector within the 0.1 cm isopach covers 6,950 km2 on land, but altogether there was some tephra fall over an area of about 40,000 km2. The tephra, which had an SiO2 content of 54-55%, was strongly polluted by fluorine, the fluorine content of the freshly fallen tephra being 800-2,000 ppm. About 1,500 ewes and 6,000 lambs were killed by fluorine poisoning. The production of lava during the first hours averaged about 800 m3/sec.

The flow from Sudurgigar ceased on 10 May, and in the Hlidargigar craters NE of the mountain on 20 May, but on the same day a new fissure 0.9 km long opened up 1 km to the north of Hlidargigar. From this fissure lava flowed incessantly until 5 July. A row of craters, now known as Oldugigar, was built up on this fissure. The highest one is about 100 m. The eruption fissures in the Sjkolkviar area are arranged en echelon, and so are seemingly the Sudurgigar eruption fissures. The total area of the 1970 lava is 18.5 km2. The lava from the Sudurgigar covers 6.5 km2, lava on the SW slopes of Hekla 2.1 km2, and the lava from the Hlidargigar and Oldugigar crater rows 9.9 km2. (Hlidargigar lava 5.8 km2, Oldugigar lava 6.6 km2, of which 2.5 km2 covered Hlidargigar lava).

The total volume of the 1970 Hekla lava is about 0.2 km3. The new Hekla lava is andesitic, containing a little olivine, and in chemical composition and texture similar to the lava produced during the last months of the 1947-48 eruption. The outer structure is typical aa lava. The chemical composition of the lava justifies the view that the 1970 eruption should be classified as a Hekla eruption, although the fissure which splits the Hekla ridge lengthwise took very little part in it. Information Contacts: Sigurdur Thorarinsson, Science Institute, University of Iceland. August 1980 (SEAN 05:08) Cite this Report Large tephra cloud and lava flows "Hekla started erupting at 1328 on 17 August. Small earthquakes were recorded on local seismographs for 20-25 minutes prior to the first explosions but these precursors were not noticed until later.

"This was a mixed eruption starting in the summit area and quickly extending to the full fissure length of 7 km, longer than observed in the 1947 and 1970 eruptions. The initial activity at 1320 was a steam column, then a dark tephra column started between 1327 and 1330. The main tephra fall lasted about 2 hours and extended NNE, and the eruption column reached about 15 km altitude. The maximum tephra thickness 10 km N of the summit was 20 cm, and at the N coast, about 230 km distant, 1 mm or less. The fluorine content in many grazing districts is above danger level, causing problems for livestock, especially sheep. Lava began flowing shortly after the beginning of the eruption. The first flows appeared near the summit, then lava eruption extended to the lower parts of the fissure. Most of the lava issued within 12 hours and nearly all within 24 hours, forming four main separate lava flows, covering an area of about 22 km2.

The volume of the lava is estimated at about 0.1 km2 and the tephra somewhat less than in the 1970 eruption, which produced 0.07 km3. "Glowing scoria was last observed in the early morning of 20 August. Steam emission was continuing as of late August. For the first few days following the eruption this steam column was often darkened at the base, but no glow was observed. "Preliminary chemical analyses of tephra and lava show composition similar to that of the 1970 eruption products. The last Hekla eruption took place 5 May-5 July 1970, making this period of quiescence of only 10 years the shortest recorded for Hekla since 1104. The shortest previous period between eruptions was 1206-22 and the second shortest was between the 1947 and 1970 eruptions. If the present eruption episode is over now, the behavior is highly unusual. All previous known eruptions have lasted from 2 months to 2 years.

Initially there have been a few days of major activity, followed by a few almost quiet days, then renewed explosive activity and lava eruption concentrated on small parts of the fissure." Information Contacts: K. Grönvold, Nordic Volcanological Institute (NVI); S. Thorarinsson, Univ. of Iceland. April 1981 (SEAN 06:04) Cite this Report Lava extrusion and ash ejection from summit crater [The report in 6:4 repeats and expands upon the preliminary information received at press time for 6:3. These reports are combined here.] An eruption of Hekla was first observed about 0300 on 9 April. The initial activity consisted of ejection of ash columns. Pilots said that ash reached 4.2 km altitude and radar registered the top of an eruption column at 6.6 km above sea level. Ash was blown N, toward the interior of Iceland, falling at least 30 km from the volcano. Lava extrusion from a newly formed summit crater began later on 9 April, reached a peak during the afternoon, then declined gradually until the eruption ended on 16 April.

Three flows were extruded, the two largest moving down the N side of the main Hekla ridge, the smallest down the S side. The lava covered an area of 5-6 km2 and extended a maximum of 4.5 km from the crater, reaching the base of Hekla Ridge on both the N and S sides. After the initial ash ejection, activity was dominantly effusive, but a small amount of ash fell E and NE of the volcano later in the eruption. The area has remained inaccessible, but ash amounts were estimated to be only a few millimeters thick. No earthquakes were recorded prior to the eruption, and distinct harmonic tremor did not appear on seismic records until after the eruption began. Volcanologists interpreted the April activity as a continuation of the much larger eruption of August 1980. Further Reference. Grönvold, K., Larsen, G., Einarsson, P., Thorarinsson, S., and others, 1983, The Hekla eruption of 1980-1981: BV, v. 46, p. 349-364. Information Contacts: K.

Gronvold, NVI; S. Thorarinsson, Univ. of Iceland. May 1981 (SEAN 06:05) SO2 detected from 1981 lava flows The COSPEC detected SO2 N and SW of Hekla's April 1981 lava flows. Information Contacts: K. Grönvold; NVI; R. Stoiber and S. Williams, Dartmouth College. January 1991 (BGVN 16:01) Cite this Report Tephra cloud to 10 km above summit; ashfalls to N coast; fluid lava flows from fissure vent [A preliminary report of Hekla's early 1991 eruption appeared in 15:12. Additional information from Agust Gudmunsson, printed in 16:1, has been added in brackets, replacing some of the original material from 15:12.] On 17 January, after 10 years of repose, an eruption ejected tephra columns and fed numerous fluid lava flows from fissure vents.

Local farmers noticed strong sulfurous smells around 1200-1300, 4-5 hours before the eruption began. Instruments, however, gave less than [30] minutes warning of the eruption. [The first earthquake associated with the eruption occurred at 1632. From 1642, the earthquakes increased in number and the largest attained M 3. Seven borehole strainmeters are located 14-45 km from Hekla, and a conspicuous strain pulse was recorded at 1636, just after the first earthquake. Volcanic tremor started at about 1700. No eruption column was detected by Icelandic Meteorological Office radar at 1700, but it had attained 11.5 km height at 1710.

The eruption column was observed from nearby farms at 1705 and 1707.] Images from the Meteosat geostationary satellite showed a plume extending NNE (azimuth 010°), over an uninhabited area, and by 2000 it was approaching the coast (more than 200 km from the volcano), where light ashfall was reported. Feeding of the eruption cloud appeared to have stopped by 2000, and the plume was clearly detached from the volcano by 2100. At 2300, Meteosat images showed a second eruption cloud, which was again carried NNE and reached 300 km in length before dissipating by 0300. Weather clouds then prevented additional satellite observations. [During the early hours of the eruption, several fissures were active, including the southern part of the main Hekla fissure.] Numerous lava flows advanced W, E, and S, extending 4-5 km by midnight. Four flank vents were visible and glow could be seen from the summit area, obscured by clouds.

Lava viscosity was relatively low, producing comparatively thin, fast-moving flows reminiscent of the 1980 eruption. [Tremor began to decrease at about 1800 and by 0400 the next morning was already down to a relatively low level. Since then it has been slowly decreasing, with occasional short-term increases. On the second day of the eruption, activity was already more or less restricted to a single fissure on the lower southern flank, trending SE from the top of the volcano. One crater on this fissure was still active as of 8 February. Slight activity could be seen in another fissure on the S side of the volcano until 20 January, but with very little lava flow and no fountains. The volume of freshly fallen tephra is estimated at roughly 0.02 km3. This is about 1/3 of the estimated volume of tephra generated during Hekla's eruptions in 1970 and 1980. The total area covered by newly erupted lava is 22-23 km2, and the estimated volume of this lava is 0.13 km3 [see also 16:3].

For comparison, the lava from the 1980 eruption covers 24 km2 and its volume is estimated at 0.15 km3. Similarly, the 1970 lava covers 18.5 km2 and has an estimated volume of 0.2 km3. The composition of the 1991 lava is very similar to that of the 1970 and 1980 lavas.] Hekla, one of the most active volcanoes in Iceland, is near the intersection of the Eastern Volcanic Zone and the transform zone of S Iceland. Although near a zone of spreading, it is not a typical rift volcano. Its products are intermediate to acid in composition. The last two repose periods (1970-80 and 1981-91) are the shortest in Hekla's known history, since 1104. Hekla's previous eruption began on 17 August 1980 and produced about 120 x 106 m3 of lava and 60 x 106 m3 of tephra before activity stopped on 20 August.

The eruption resumed on 9 April 1981, extruding another 30 x 106 m3 of lava in the succeeding week; [these two episodes are usually regarded as a single eruption] (Grönvold and others, 1983). Reference. Grönvold, K., Larsen, G., Einarsson, P., Thorarinsson, S., and Saemundsson, K., 1983, The Hekla eruption 1980-1981: BV, v. 46, p. 349-363. Information Contacts: P. Einarsson and S. Björnsson, Univ of Iceland; [A. Gudmunsson and] E. Tryggvason, NVI; O. Karst and J. Paquette, NOAA. March 1991 (BGVN 16:03) Cite this Report Lava effusion ends in early March "The eruption that started on 17 January (15:12 and 16:1) lasted until 11 March, or nearly 53 days.

The eruption produced mainly basaltic andesite lava, with a total area of about 23 km2. Its thickness is as little as 2 m on the steepest slopes of the volcano but exceeds 10 m on flat ground. The estimated average thickness is 6-7 m and the volume of lava is 0.15 km3. The volume of freshly fallen tephra is estimated as roughly 0.02 km3 but negligible when calculated as dense lava. Consequently, 0.15 km3 may be regarded as the total volume produced during this eruption. The lava and tephra are basaltic andesites, almost identical in composition to those produced in the eruptions of 1970 and 1980-81. "Changes in the volcanic tremor, as well as field observations, indicate that the main eruption occurred from 1700 on 17 January to about 0400 on 18 January. During this period the effusion rate may have attained 2,000 m3/s, but the average production of lava during the first 40 hours of the eruption was ~800 m3/s.

After attaining its peak on the first day, the effusion rate decreased rapidly to ~10 m3/s. The rate then decreased slowly during the next three weeks to a temporary minimum of ~1 m3/s on 9 February. The effusion rate increased again on 14 February and was ~10 m3/s on 16 February. The rate decreased to ~3 m3/s on 24 February, to ~1 m3/s on 6 March, and then remained similar until the end of the eruption." Further Reference. Gudmundsson, A., Oskarsson, N., Grönvold, K., Saemundsson, K., Sigurdsson, O., Stefansson, R., Gislason, S., Einarsson, P., Brandsdottir, B., Larsen, G., Johannesson, H., and Thordarson, T., 1992, The 1991 eruption of Hekla, Iceland: BV, v. 54, p. 238-246. Information Contacts: A. Gudmundsson, NVI.

February 2000 (BGVN 25:02) Cite this Report Fissure eruption; abundant lava flows produced On 26 February 2000 the WSW-trending, elongated Hekla volcano erupted. A fissure 6-7 km long opened along the SW flank of the Hekla ridge, from which a discontinuous curtain of lava erupted starting at 1819. Just a few minutes later, at 1825, an ash plume reached a height of 11 km and was carried N by light winds. Based on the tremor amplitude the eruption reached peak intensity in the first hour of activity, then gradually declined. Seismic networks maintained by the Science Institute at the University of Iceland and the Icelandic Meteorological Office recorded short-term precursors. Small earthquakes were first detected by seismographs at various locations during 1655-1707. These gradually increased and the first well-located earthquakes (M 1-2) started at 1729, centered 1-2 km SE of the summit at depths of a few kilometers.

A network of borehole strainmeters operated by the Meteorological Office also detected precursory changes associated with magma movements. A decrease in strain build-up rate, signaling a release of magma pressure, was recorded by a strainmeter in a borehole ~15 km from the summit at 1817. Notice was given to the National Civil Defense and the Civil Aviation Administration about 40 minutes before the eruption, and the public was alerted about the imminent eruption about 15 minutes before it began through national radio broadcasts. Continuous low-frequency tremor began at 1819, at the same time the eruptive cloud was spotted. Ashfall was reported on 26 February from Grimsey Island, ~70 km off the N coast of Iceland and 300 km N of Hekla. Although small amounts of ash fell in inhabited areas of N Iceland, most fell in uninhabited areas of the island's interior. Seven hours after the eruption's onset the ash deposit 21 km N had a maximum thickness of 4-5 cm. Lava flows on 27 February covered a large part of the SE flank.

That evening a lava stream flowed N from the erupting fissure at a rate of several meters per hour. Another more active lava stream emanated from three craters near the S end of the fissure; the stream was several kilometers long and advancing at ~1 m/minute. On 28 February an eruption cloud was deflected towards the S by northerly winds. However weather conditions precluded direct observations. Tremor amplitude continued to slowly decline, and the strength of the eruption was decreasing (figure 1). Two eruption clouds were seen at 0500, confirming that activity was ongoing. Although the craters were not visible in the daylight, the most active crater just S of the summit produced three lava streams down the S flanks. Activity in the N declined during the day on 28 February. At 0630 one lava flow had reached the Vatnafjoll mountains at Lambafell, 5 km S of the summit. Advancing at ~2-3 m/hour, the lava front was estimated to be 8-10 m wide. That evening observers watched Strombolian activity in three craters at the southernmost part of the fissure. Figure 1.

Tremor at Hekla during 26-28 February 2000 recorded at Haukadalur, 10 km W. At the beginning of the eruption, 1819 on 26 February, the tremor increased rapidly and reached a maximum at 1850. Tremor then decreased until about 0700 on 27 February and became steady. The tremor was approximately 10 % of the maximum value, on 28 February, but over 10 times greater than the normal value. Courtesy of Páll Halldórsson, Science Institute at the University of Iceland. Ashfall was reported on the morning of 29 February 35-40 km S in Fljótshlíð. At 0500 volcanic tremor had started to increase and continued until 1000-1100. By about 0800 all activity in the summit had ceased. During the afternoon of 29 February activity at the southernmost end of the fissure increased again, producing eruption clouds ascending above the summit.

In the darkness of the evening, three craters at the southernmost end of the fissure produced lava flowing SW. People watching the lava on the NE flanks reported that they could walk on the stopped flow there. Vigorous Strombolian eruptions and lava flows on the fissure that cuts the SW slopes were seen during a reconnaissance flight on 1 March during 1100-1230. Four main vents and three smaller vents produced explosions at intervals of 4-5 minutes. At the base of the fissure a large tumuli had developed. The lava streams coming out through the opening of the tumuli joined a stream coming from overflows of the uppermost craters. The S-directed lava flows were fed by the crater closest to the summit. The lava field in the S had only advanced ~100 m since 28 February, but on 1 March it was growing toward the E. By 1 March lava had covered approximately 17 km2. Increased activity was observed in the upper craters on 2 March, although bad weather persisted from 1200 on 1 March until midday on 3 March.

There was also constant steaming from the SW craters, and, compared to 1 March, much larger steam clouds rising from the upper craters. At nightfall explosions were observed at ~30-minute intervals. Glowing lava streams were noted on the flank of the mountain on 2 March. On 3 March a group of scientists reached the SW lava flow at 1300 and found that the lava front was ~10 m wide and advancing very slowly, ~1-2 m/day. While tracing the lava to the W the group noted that at some places the flow was spreading much faster, up to ~1 m/hour. Following the lava flow along its W side, the group reached its origin at the foot of the volcano, where it emerged from the end of the erupting fissure. At the origin, the estimated flow rate was 0.06 m/s, producing about 10 m3/s of lava. Due to the continuous degassing along the lava stream a blue mist was formed. The blue mist was also observed farther E along the flank of the volcano, indicating that lava was still flowing from the crater close to the summit area.

The craters in this region fed the lava flow that moved S toward the Vatnafjoll glacier 10 km SE from Hekla. Later in the evening observers reported that lava was still flowing slowly towards Vatnafjoll. Explosive activity in the uppermost crater of the SW-fissure was characterized by small explosions at 10-20 minute intervals that produced white steam clouds with only trace amounts of ash. Due to bad weather conditions on 4 March, no direct observations could be made of the eruption. Decreasing eruption tremor was detected. On 5 March the lava flow to the SW was still ongoing according to observations made in the afternoon. At sunset, a red pulsing glow was observed in the uppermost craters of the SW-fissure from the town of Selsundsfjall, 15 km SW. Small eruption clouds were observed on 6 March penetrating the weather clouds covering the summit of Hekla. During a reconnaissance flight between 1730 and 1830 on 6 March the whole fissure was steaming vigorously and all of the lava flows appeared to have stopped. The lava stream in the SW had left behind an empty channel.

Neither incandescence nor explosive activity were observed from the craters. Minor tremors continued on 6-7 March, but may have been related to lava degassing in the feeder dike. At 0844 on 8 March the last eruptive tremor was detected on seismometers. Based on the end of detectable tremor, and with no signs of new eruptive products since 5 March, it was determined that the eruption ended on the morning of 8 March. Lava covered approximately 18 km2; the preliminary estimate of lava production was 0.11 km3. Plume investigation. Sulfur dioxide (SO2) contained in plumes from Hekla was detected by the Earth Probe TOMS (Total Ozone Mapping Spectrometer) instrument. TOMS imagery at 1154 on 27 February showed that the volcanic cloud was a narrow plume arcing from the volcano in southern Iceland, then N to Greenland, and finally E towards Norway. The plume primarily contained SO2 because almost all of the ash fell out locally. On 28 February the TOMS imagery indicated that plume stretched out over the Barents Sea and possibly into eastern Russia.

By 29 February the SO2 cloud had drifted E in a band along the Norwegian and Russian coasts of the Barents Sea. During a transit flight on 28 February a SOLVE (SAGE III Ozone Loss and Validation Experiment) mission with an instrument-laden DC-8 aircraft flew through the plume shortly after the eruption ~11.3 km NNE of Iceland at 76°N and 5°W, just off the Greenland coastline. The plume extended up to ~13 km altitude, well into the lower stratosphere. Instruments also measured many in situ trace gases, SO2, HNO3, NO, NOy, O3, and aerosols (volatile and non-volatile), including their size distribution. From about 0508 until 0518 on 29 February the SOLVE aircraft again entered the volcanic cloud. The scientific team reported large enhancements in CN, NOy, HNO3, CO, and particle counts, ozone went to nearly zero, H2O jumped up, and there were strong scattering layers up to 13 km. The plume was a very impressive, orange, airfoil-shaped feature in the pre-dawn sky.

The DC-8 engines needed an oil change and new filters after passing through the plume. A flight on 5 March detected enhanced aerosols and SO2 at 1301, but by that time the plume was so diluted that it represented no danger to the aircraft. During the three weeks following the initial encounter the DC-8 detected remnants of the plume trapped within the polar vortex. The resulting analysis concluded that volatile aerosols increased and the sizes of non-volatile large aerosols decreased. Fluoride analysis. Ash from previous Hekla eruptions has often been the cause of fluorosis in grazing animals. However, during this time of the year most domestic animals are kept indoors, so fluorosis is not expected to become a problem. Freshly fallen ash was measured for soluble fluoride ions (F-). The result was 800-900 mg F/kg. Snow melted by the ash contained about 2,200 mg/l (ppm) of fluoride.

Information Contacts: Freysteinn Sigmundsson, Nordic Volcanological Institute, Grensásvegur 50, IS-108 Reykjavik, Iceland (URL: Email: fs@norvol.hi.is); Páll Einarsson, Science Institute, University of Iceland, Hofsvallagata 53, IS-107 Reykjavík, Iceland (Email: palli@raunvis.hi.is); Ragnar Stefánsson, Icelandic Meteorological Office, Bustadavegur 9, 150 Reykjavík, Iceland (URL: Mark Schoeberl, Code 910, NASA/GSFC, Greenbelt, MD, 20771 USA (URL: Email: Mark.Schoeberl.1@gsfc.nasa.gov); Michael Fromm, Computational Physics, Inc., 2750 Prosperity Ave., Suite 600, Fairfax, VA 22031 USA (URL: solve/, Email: fromm@poamb.nrl.navy.mil); Arlin Krueger, Code 916, NASA/GSFC, Greenbelt, MD, 

20771 USA (Email: krueger@chapman.gsfc.nasa.gov).

June 2000 (BGVN 25:06) Cite this Report Clarification of NASA airborne plume experiments on 29 February 2000 NASA's Dryden Flight Research Center (DFRC) advised that information concerning two flights of their DC-8 aircraft as reported in BGVN 25:02 contained errors and requested that the information be corrected with additional details as follows: "For approximately seven minutes starting at 0510 during a transit flight on 29 February to Kiruna, Sweden, a NASA DC-8 aircraft with a payload of SOLVE (SAGE III Ozone Loss and Validation Experiment) sensors flew through the plume ~11.3 km NNE of Iceland at 76 °N and 5 °W, just off the Greenland coastline. The plume extended up to ~13 km altitude, well into the lower stratosphere. The aircraft passed thorough the volcanic ash far N and W, and at a flight level much higher, than the predictions reported by the Volcanic Ash Advisory Center (VAAC), London.

Instruments measured many in situ trace gases, SO2, HNO3, NO, NOy, O3, volatile and non-volatile aerosols, and aerosol size distribution. The scientific team reported substantial increases in CN, NOy, HNO3, CO, and particle counts, O3 went to nearly zero, H2O increased, and strong scattering layers up to 13 km were detected. "A flight on 5 March detected enhanced aerosols and SO2 at 1301, but by that time the plume was so diluted that it represented no danger to the aircraft. During the three weeks following the initial encounter the DC-8 detected remnants of the plume trapped within the polar vortex. The resulting analysis concluded that volatile aerosols increased and the sizes of non-volatile large aerosols decreased." NASA-DFRC also advised that the statement about the plume being a "very impressive, orange, airfoil-shaped feature in the pre-dawn sky" was erroneous. Post-flight interviews with the pilot indicated that there was no moon out, therefore pitch black sky conditions existed at the time of the encounter. The pilots had no visual evidence of flying into the plume.

Information Contacts: Gary Shelton, NASA, Dryden Flight Research Center, P.O. Box 273, Edwards, CA 93523-0273 USA. September 2014 (BGVN 39:09) Cite this Report Elevated seismicity during March-April 2013 Introduction. This Bulletin report covers the unusual seismic activity recorded at Hekla from early March through April 2013. The last Bulletin report (BGVN 25:06) on Hekla clarified errors concerning NASA’s airborne plume experiments on 29 February 2000, which occurred during Hekla’s last eruption. Several references have been included to provide more information on Hekla’s most recent eruptions in 1991 and 2000. Below are also two maps showing Hekla’s location and lava flows created during some of Hekla’s eruptions (figures 2 and 3). Figure 2. Map highlighting Hekla’s location in Iceland. Hekla is located at the juncture where the E volcanic zone, a propagating rift, meets the South Iceland seismic zone, a transform fault.

Source: Gudmundsson and others (1992). Figure 3. Map highlighting lava flows created through Hekla’s past eruptions. The map also identifies GPS stations (triangles) and tilt sites (square) used to monitor Hekla. Some stations are operated by the Icelandic Meteorological Office (IMO) and others are operated by Penn State University in collaboration with IMO. The yellow lines represent Hekla’s fissure, Heklugjá. Map was on found on University of Iceland’s Institute of Earth Sciences website; credit to Sigrún Hreinsdóttir. March 2013. On 10 March 2013, the Icelandic Meteorological Office (IMO) began detecting micro-earthquakes at Hekla. The IMO detected at least 7 high-frequency earthquakes whose magnitudes ranged from 0.4-1. The earthquakes were recorded over a small area approximately 4.5 km to the NE of Hekla’s summit with a source 11-12 km below the surface. The earthquakes were judged as the result of brittle fracture rather than a consequence of magma moving.

It is important to note a clustering of earthquakes such as these is uncommon during non-eruption periods at Hekla. The IMO informed the National Commissioner of the Icelandic Police (NCIP) of the occurrence of these earthquakes. This type of activity had not been seen since Hekla’s last eruption. With this information the NCIP and the Police Commissioner at Hvolsvöllur declared an ‘uncertainty phase’, which is the lowest of three warning level regarding natural hazards. The IMO also changed the Aviation Colour Code from Green to Yellow. The Aviation Colour Code is a 5-level color code scale that informs the aviation community of a volcano’s status. The 5 levels in order of increasing volcanic activity are Grey, Green, Yellow, Orange and Red. According the IMO website, the Yellow color code signifies that a “volcano is experiencing signs of elevated unrest above known background levels or, after a change from [a] higher alert level…” On 28 March, no seismic activity was detected at Hekla for ~4 days. No obvious signs of an imminent eruption were reported. Nevertheless, the ‘uncertainty phase’ warning level was kept in effect and the Aviation Colour Code remained Yellow.

For the last few days of March 2013, no new activity was reported. April 2013. For the first three days of April, Hekla remained quiet, but the ‘uncertainty phase’ warning level remained in effect. On 4 April, the IMO changed the Aviation Colour Code from Yellow to Green. No changes in gas or heat were observed at Hekla’s summit and no crustal movement was detected. Due to the low activity, the ‘uncertainty phase’ warning level was removed. Hekla continued to be quiet until 26 April, when an M 1.1 earthquake occurred in the same area as the earthquakes in March. No other activity was reported at Hekla for the rest of April. References.

Aviation Colour Code map, Icelandic Meteorological Office, date accessed 17 March 2015, (URL: ) Gudmundsson, A., Oskarsson, N., Grönvold, K., Saemundsson, K., Sigurdsson, O., Stefansson, R., Gislason, S., Einarsson, P., Brandsdottir, B., Larsen, G., Johannesson, H., and Thordarson, T., 1992, The 1991 eruption of Hekla, Iceland, Bulletin of Volcanology, v54, pp 238-246, date accessed 16 March 2015 (URL: ) Hekla volcano 2013-daily reports, Trip to Iceland, 27 March 2013, date accessed March 17, 2015, (URL: ) Höskuldsson, Á., Óskarsson N., Pedersen, R., Grönvold, K., Vogfjörð, K., and Ólafsdóttir, R., 2007, The Millennium

 Eruption of Hekla in February 2000.

Bulletin of Volcanology, v70 (2), pp 169-82, DOI 10.1007/s00445-007-0128-3, data accessed 16 March 2015 (URL: # ) Seismic activity in Mount Hekla, Icelandic National Broadcasting Service (RUV), 26 March 2013, date accessed 17 March 2015, (URL: Soosalu, H.

and Einarsson P., 2001, Earthquake Activity Related to the 1991 Eruption of the Hekla Volcano, Iceland, Bulletin of Volcanology, v63(8), pp 536-544, DOI 10.1007/s00445-001-0177-y, date accessed 16 March 2015 (URL: # ) Soosalu, H., Einarsson, P., and Jakobsdóttir, S., 2003, Volcanic tremor related to the 1991 eruption of the Hekla volcano, Iceland, Bulletin of Volcanology, v65, pp 562-577, DOI 10.1007/s00445-003-0285-y, date accessed 16 Mar 2015 (URL: #page-1) Soosalu, H., Einarsson P., and Þorbjarnardóttir, B.

S., 2005, Seismic Activity related to the 2000 Eruption of the Hekla Volcano, Iceland, Bulletin of Volcanology, v68(1), pp21-36, DOI 10.1007/s00445-005-0417-7, date accessed 16 March 2015 (URL: Information Contacts: Icelandic Meteorological Office, Bustadavegur 7-9, 108 Reykjavík, Iceland (URL: ); National Commissioner of the Icelandic Police (NCIP), Civil Protection and Emergency Management Department, Skúlagata 21, 101 Reykjavík, Iceland (URL: and Sigrún Hreinsdóttir, GNS Science, PO Box 30368 1 Fairway Drive, Lower Hutt, 5010 New Zealand (URL: Basic Data Hekla | Guide to Iceland View Hjálparfoss Hjalparfoss is one of several waterfalls in Thjorsardalur valley, north of the volcano Hekla, in south Iceland.

This is a two-stepped waterf... View Þjórsárdalur Thjorsardalur is the easternmost valley of Arnessysla in South Iceland. The valley is lush and contains amazing natural and cultural attractions. Thj... View Þjódveldisbærinn á Stöng At Stong in Thjorsarsalur valley in South Iceland you can see the Thjodveldisbaer, a reconstructed viking turf house based on the ruins of the old man... Hólaskógur Holaskogur is an deforested area (despite the name, 'skogur'='forrest') in Gjupverjaafrettur in the mid highlands of Iceland.&... View Háifoss Haifoss ('High Waterfall') is a waterfall in Fossardalur valley, innermost of Thjorsardalur valley in South Iceland. Haifoss is held ... View Tindafjallajökull Tindafjallajokull is a volcano, submerged by a glacial ice cap. It is located northwest of Thorsmork. The glacier covers about 19 km2....

View Brennisteinsalda Brennisteinsalda (ca. 855 m) is a volcano in the area of Landmannalaugar National Park, in the south highlands of Iceland. Brennisteinsalda ... View Dómadalur Domadalur is a valley east of Kringla (Landmannahellir cave) in the south of the Icelandic highlands. The valley has a little shallow lake a... View Laugavegur hiking trail The Laugavegur is one of the most popular hiking trails in Iceland. The scenery is breathtaking in its beauty and extremely varied, displaying example... View Bláhnjúkur Blahnjukur (a.k.a. Blahnukur) is a volcano in the area of Landmannalaugar, in the south highlands of Iceland. Blahnjukur's name (&#... View Landmannalaugar Landmannalaugar ("The people's pools") is a wast area of stunning beauty in Iceland's Southern Highlands. This unique geologi...

View Bláfjöll The Blue Mountains are a beautiful mountain range of the tuff type, located around 20 km from Reykjavik, by the lava plateau of Hellisheidi. T... View Hrepphólar Hreppholar is a series of regular basalt columns located at Hrunaheidi heath in South Iceland. These towering pillars are located at the Hrunaheidi h... View Ljótipollur Ljotipollur is a explosion crater lake in the south highlands, situated in the southernmost crater in the Veidivotn fissure system. Strangely... View Stakkholtsgjá Stakkholtsgja is an up to 100 meters deep and 2 kilometers long canyon in South Iceland. The canyon is located near the entrance to Tho... View Fljótshlíð Fljotshlid is a beautiful farming district in southern Iceland. It is one of the main sites for Njal's Saga, a masterpiece of the saga lit... View Hvolsvöllur Hvolsvollur is a small town of 800 people in South Iceland, conveniently located by the ring road.

The local airport has flights to the Westman Island... View Miðás Breeding Farm Midas is a horse farm near Hella in South Iceland. The farm is run by farmers Asta Begga Olafsdottir and Gisli Sveinsson. It features a stable, a r... View Stóra-Laxá Stora-Laxa is a 90 km long fresh water river, located at Hreppar in South Iceland. It is renowned for its salmon and widely considered one of Iceland&... Hekla Volcano Tour Iceland – Arctic Adventures Terrain: Rough lava fields, ice, and snow as the peak draws nearer. Average ascend time: 3-4 hours. Total average trip time: 7-8 hours (12 hours with pick up & drop off). Height gain: ~1040 meters. Mt. Hekla is undeniably one of Iceland’s most famous volcanic mountains. It is the second most active volcano in Iceland and has erupted many times in the past, including once in February 2000. The mountain towers over South Iceland at roughly 1491 meters and its height changes due to seismic movements and the shifting of the earth’s crust.

Eggert Ólafsson, a famous Icelandic biologist, decided to throw caution to the wind and eventually succeeded in being the first to summit the mountain in the summer of 1750. Since then hiking to the top of Mt. Hekla has become one of the most popular routes on the island. However, it is not recommended to drive up its sides as the timeframe between the signaling earthquakes and an eruption is only 30-60 minutes. The view from the top of Mt. Hekla is widespread and beautiful; you have the opportunity to get a clear sight of the Fjallabak mountains, up to Vatnajökull glacier, (Europe’s biggest glacier) and all of the evidence of recent and longstanding volcanic activity.We reserve the right to postpone or cancel trips due to weather or other factors out of our control. Click here for our cancellation policy. The Great Volcanoes: Hekla | Iceland Review The Great Volcanoes: Hekla Updated: September 22, 2014 22:23 Heaven and Earth erupt simultaneously. Photo: Sigurður Hrafn Stefnisson.

Even though the Holuhraun eruption is already one of the biggest eruptions in Iceland in recent history, and has caused many inconveniences, it is still not among the most dangerous ones. But as we have often explained, it might turn into one. In this and further articles, we will talk about some of the most famous and dangerous Icelandic volcanoes. The paradox of an eruption is that it can be beautiful and destructive at the same time. The most famous volcano in Iceland, historically speaking, is probably Hekla. It was known in medieval texts as the 'Entrance to Hell.' The 1104 eruption caused great damage and wiped out whole districts, including upper Þjórsárdalur. Since then there haven't been any farms in that area. The earliest recorded eruption in Hekla took place in 1104. Since then there have been between 20 and 30 considerably large eruptions, with the volcano sometimes remaining active for periods of six years with little pause. Eruptions in Hekla are extremely varied and difficult to predict.

Some are very short (a week to ten days), whereas others can stretch into months and years (the 1947 eruption started March 29 and ended in April, 1948). But there is a general correlation: the longer Hekla stays dormant, the larger and more catastrophic its opening eruption will be. The most recent eruption was on February 26, 2000. This amazing photo by Sigurður Hrafn Stefnisson shows two interesting phenomena: The northern lights and the eruption in Hekla in 1991. You can find many more of his photos at . Related Hekla volcano, Iceland HEKLA ERUPTS AGAIN AFTER 9 YEARS !! 8 March 2000 As reported by NORDVULC, the eruption is now considered to be over. The last weak volcanic activity occurred on 5 March, and the last tremor signal on 8 March. The eruption emplaced about 0.11 km3 of lava, mostly as flows covering an area of about 18 km2. 1 March 2000 As reported by the newspaper Morgunbla�i� , the eruption has again increased in intensity.

This time, ash was transported westwards and fell on Rejkjavik but did not cause damage. The area covered by lava flows is now estimated to be 16-18 km2. 27 February 2000 In the evening of February 27 the main lava flow from the eruptive fissure was slowly advancing at a rate of some meters per hour. A more active lava stream emanates from three craters near the southern end of the eruptive fissure. On February 27 this lava stream was several km long and was advancing at a rate of about a meter per minute. 26 February 2000 Hekla volcano in South Iceland erupted after a repose interval of just 9 years on February 26, 2000 at 18:19 GMT. Initially, a 6-7 km long eruptive fissure opened up along most of the Hekla ridge. A discontinuous curtain of fire emanated from the whole fissure. A more than 10 km high ash plume formed within few minutes of the explosive beginning of the eruption.

The ash was carried with light winds towards north and most of it fell in uninhabited areas in the interior of Iceland, but a small amount of ash fell in inhabited areas in North Iceland. After the first hour the activity gradually declined and soon became predominantly effusive. map of post-1970 lava flows from Hekla volcano. Hekla Volcano, Iceland - John Seach summit elevation 1491 m stratovolcano Hekla Volcano is located in southern Iceland 110 km east of Reykjavik, and 55 km from the coast. Hekla is the most active volcano in Iceland, and one of the world's best known volcanoes. Hekla volcano, Iceland - John Seach The structure of Hekla is considered intermediate between crater row of Laki-type, and stratovolcano of the Vesuvius-type. It is built on a 5 km long fissure. Repose periods at the volcano have lasted from 10 to 102 years. The magma reservoir feeding Hekla is located at a depth of 5-9 km. During non-eruptive periods the volcano is virtually aseismic.

Eruption-related seismicity starts only 30-80 minutes before its onset. Hundreds of small volcano-tectonic earthquakes (magnitude < 3), related to the intrusion of magma, occur during the first hours, when the eruption is violent and explosive. Since 1970, Hekla volcano has erupted about every 10 years. The initial phase of each Hekla eruption is always highly explosive. The duration and magnitude of the explosive phase is directly correlated with the length of the preceding repose period. 2013 Unrest A level of uncertainty was declared at Hekla volcano on 26th March 2013 due to an increase in sesimic activity. 2000 Eruption Changes in groundwater table were observed up to 2 years before the eruption started. A short-lived but intense eruption of Hekla volcano began on 26th February 2000, and lasted for 12 days. A 6.6-km-long fissure opened along the length of Hekla volcano from the SW to the NE, south of the summit area. A Subplinian eruption plume reached a height of 12 km in 32 minutes.

This was accompanied by several small pyroclastic flows. Volcanic activity at Hekla changed to fire fountaining and then to Strombolian, ending with a quiet effusive lava phase. 1991 Eruption An eruption started at Hekla volcano at 5 p.m. (UT) on 17th January 1991.The eruption column reached a height of 11.5 km in 10 minutes. Ten hours after the start of the eruption, an eruption plume extended 300 km from the volcano. During the first few hours of the eruption, lava fountains rose to a height of 300 m. By the second day of the eruption, the activity was already more or less restricted to a single fissure on the lower south flank trending southeast from the summit of Hekla. Effusion of lava was strongest in the first 11 hours of the eruption. During the first couple of weeks, a single lava flow effused from the crater. Subsequently, however, it flowed in a tube for a few hundred metres from the crater and then to the surface through five vents. Lava flows covered 23 sq km.

The eruption declined on 23rd February 1991. Like the 1970, and 1980-81 eruptions, the 1991 eruption at Hekla issued from flank fissures rather than the summit fissure. 1980-81 Eruption On the day of the eruption, campers 10 km north of Hekla noticed a sulphur smell, and birds (geese and golden plovers) were restless. The eruption began at Hekla volcano on 17th August 1980 with a plinian phase and simultaneous emission of lava from a fissure along the Hekla volcanic ridge. The eruption began at 13:25 or 13:30 hr, and by 14:00 hr the eruption column reached a height of 15 km. The eruption rate declined rapidly after the first day and the eruption stopped on 20th August. The August 1980 eruption at Hekla came without warning. No earthquakes had been found to originate in the vicinity of the volcano for at least several years, in spite of a relatively dense seismograph network near the volcano.

Like the 1970 eruption, the 1980-81 eruption at Hekla issued from flank fissures rather than the summit fissure. 1970 Eruption The 1970 eruption at Hekla was unusual up until this time, because it occurred from the flank and base of Hekla ridge, rather than the usual main fissure system. On 5th May 1970 earthquakes up to magnitude 4 were registered at Reykjavik. Several hours before the earthquakes started, dog were restless at Burfell hydropowerstation, 15 km NW of Hekla. The eruption began at 21:23 hr when fissures opened up nearly simultaneously on the SSW and W flanks of the Hekla ridge. Two craters opened up on the SSW-flank, at an elevation of 800 m, followed by a third crater at 780 m. A 1000 m high lava fountain erupted from the third crater at 22:30 hr.

A little over an hour after the eruption started in the SW part of Hekla, an eruption began NNE of the Hekla ridge, at a distance of 7 km from the first eruption site. Fluorine poisoning killed thousands of grazing livestock, especially sheep, in west Hunavatnssysla and parts of Arnessysla. By 20th of May fluorine content of the tephra had decreased and the grazing land became safe for livestock. In the first 10 hours of the eruption, lava flows covered an area of 7.5 sq km. 1947-48 Eruption Hekla volcano began erupting on 29th March 1947. At 6:51 am, a large earthquake centered at the volcano was felt 150 km away. Shortly afterwards a 5 km long fissure opened along Hekla ridge. People 300 km away were awakened by the roar of the explosions. By 7 o'clock the ash column reached 27 km high (90,000 ft).

During the two first hours of the eruption about 180 million cubic meters of ash, pumice, bombs and scoria were erupted from the fissure. The British ship "Sacramento" located 820 km south of Hekla in the Atlantic Ocean reported ashfall of 30 tons per square kilometer. Ash from Hekla was transported in the upper layers of the troposphere to Finland, where it began to fall about 40 hours after the eruption had begun. The main ashfall lasted about 2 hours. The initial phase of the eruption was Plinian type, then changed to Vesuvian type. Eruptions decreased during the second day. On 3rd May, 5 weeks after the beginning of the eruption, the explosive activity of the craters changed to almost continuous emission of black, fine grained ash, which persisted for the next two months. At the SW end of the fissure, lava flowed from a vent for 13 months, ending on 25th April 1948. 1766 Eruption The largest known lava eruption at Hekla began on 5th April 1766.

The eruption was preceded by a decrease in outflow from springs. 1104 Eruption An eruption at Hekla volcano in 1104, devastated the inhabited Thjorsardalur valley. The eruption produced 2.5 cubic km of tephra, which was carried towards NNW. An eruption plume reached a height of 36 km. The eruption of 1104 is the only one where no lava flows formed. This was the first eruption at Hekla volcano for 250 years.

Hekla Volcano Eruptions 2000, 1991, 1980-81, 1970, 1947-48, 1913, 1878, 1845-46, 1766-68, 1725, 1693, 1636-37,1597, 1554, 1510, 1389-90, 1341, 1300-01, 1222, 1206, 1158, 1104 Hekla - Iceland On The Web Iceland On The Web Hekla Hekla is Iceland’s most famous volcano An active volcano for centuries, the mountain Hekla is one of the most famous in the world. Hekla is a stratovolcano, located near the southern end of the eastern rift zone in Iceland. The whole mountain ridge of Hekla is about 40 km long.

The fissure, Heklugjá, which splits the ridge, is about 5.5 km long. The mountain is about 1, 491 m high. During historical times, frequent large explosive eruptions have deposited tephra throughout Iceland, which provide time markers used to date eruptions from other Icelandic volcanoes. The legend of Hekla Old tales tell of the belief that the souls of the condemned travelled through Hekla's crater on their way to Hell. Others say that the witches met with the devil on its top. It has been compared with Brocken and Vesuvius and the trio were thought to be the gateways down to Hell. Through the centuries, Hekla had achieved renown of almost mythical proportions – so much so, that when a German cartographer of the 16th century drew a new marine map of the Nordic countries, on the map of Iceland which he created, there was only one proper name: Hekl’berg (Hekla). Hekla’s notoriety continued through the next three centuries, the volcano appearing as a symbolic entity in the works of several European authors.

The European name for Hekla was “Hekkenfeld”, the name that the great Icelandic Nobel Laureate Halldór Kiljan Laxness also used in his novel Iceland’s Bell (set at the close of the 17th century). When the novel´s protagonist Jón Hreggviðsson turns up in Holland, he quickly discovers that: “Everyone in Holland was familiar with Hekkenfeld in Iceland, under which burn the fires of Hell, and they were very eager to hear tales of this mountain. They called the man van Hekkenfeld.” Hekla volcano - eruption history It is thought that Hekla has had at least twenty eruptions since the settlement of Iceland in the year 874 AD. The biggest eruption was in 1104 AD when it erupted without warning ejecting millions of tonnes of tephra. It erupted four times in the 20th century, the last time in 2000. Hekla has erupted more often than any other volcano in Iceland. Some eruptions have been so powerful and violent that the volcanic ash reached as far as mainland Europe.

In the 1947 eruption, the last really big one, 14 m (46 ft) were added to its summit. In that eruption the volcano spewed up a column of ash as high as 28,000 metres into the atmosphere, and 51 hours after the eruption had started, volcanic ash from Hekla fell on Helsinki, having covered a distance of 2,860 km in this time. Eruptions of Hekla are extremely varied and difficult to predict. Some are very short (a week to ten days) whereas others can stretch into months and years. The 1947 eruption that started on 29 March 1947 ended in April 1948. The quiet (or repose) period between Hekla's eruptions has ranged from 16 years to 121 years. A tendency toward longer repose intervals has occurred between the later eruptions. Over the past 7000 years Hekla has had 5 big fissure eruptions. The biggest eruptions were 4000 and 2800 years ago.

Traces of these two eruptions can be found in the soil in the north and the north-east of Iceland. The biggest layer of tephra from one eruption fell during the eruption 2800 years ago. It covers about 80% of the country and its volume was around 1.2 cubic km. Traces of it have been found in various places in Scandinavia. Over the last millennium, Hekla has produced one of the largest volumes of lava in the world, around 8 cubic km. Year Is Iceland’s Hekla volcano going to erupt? Is Iceland’s Hekla volcano going to erupt? Duration: 00:49 EMAIL Alamy The volcanoes of Iceland are some of the most closely watched on the planet. Not only is there an extensive seismic array that records all the earthquakes that occur on the island nation, but many volcanoes have both GPS monitoring of their shape and borehole strain gauges that measure stresses underground caused by these changes in shape. READ MORE Hekla | volcano, Iceland | Britannica.com volcano, Iceland Alternative Title: Mountain of Hell Similar Topics Teide Peak Hekla, active volcano , southern Iceland , lying within the country’s East Volcanic Zone.

It is Iceland’s most active and best-known volcano. The volcano is characterized by a 3.4-mile- (5.5-km-) long fissure called Heklugjá, which is active along its entire length during major eruptions. Lava flows issuing from this fissure have contributed to the volcano’s elongated shape. Hekla stands 4,892 feet (1,491 metres) above sea level 70 miles (110 km) east of Reykjavík , the capital, at the eastern end of the island’s most extensive farming region. Hekla volcano, southern Iceland. © Ihervas/Shutterstock.com Known in early times as the Mountain of Hell, it erupted more than 20 times between 1104 and 2000, with major eruptions occurring in 1300, 1766, and 1947–48. The 1766 explosion caused great loss of life. The eruption of 1947–48 lasted for 13 months and sent an ash cloud nearly 16 miles (27 km) into the atmosphere; ash fell as far away as Finland.

Since the late 20th century Hekla’s eruptions have been characterized by an explosive ash-producing phase that precedes or occurs simultaneously with fountaining or flowing lava. Hekla had four minor eruptions during this time: in 1970, 1980, 1991, and 2000. The eruption in 2000 lasted four days but caused no significant damage. Volcanoes and glaciers of Iceland. Encyclopædia Britannica, Inc.

Question: The volcano Hekla is on which island?
Answer: Iceland